Abstract
We will consider the stochastic Navier–Stokes equation for the swirling flow(1.23), see Sect.1.4, in the next three sections. Similar results hold for the stochastic Navier–Stokes equation(1.65) describing fully developed turbulence. However, to emphasize that (1.23) and (1.65) are not the same equations we will set the coefficients c k to c k =h k in (1.23) below. The h k s can then be large but decay with increasing k. In this section we will first explain the probabilistic setting and prove some a priori estimates.
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4.1 Leray’s Theory
We will consider the stochastic Navier–Stokes equation for the swirling flow (1.23), see Sect. 1.4, in the next three sections. Similar results hold for the stochastic Navier–Stokes equation (1.65) describing fully developed turbulence. However, to emphasize that (1.23) and (1.65) are not the same equations we will set the coefficients c k to c k = h k in (1.23) below. The h k s can then be large but decay with increasing k. In this section we will first explain the probabilistic setting and prove some a priori estimates.
We let (Ω, ℱ, ℙ), Ω is a set (of events) and ℱ a σ-algebra on Ω, denote a probability space with ℙ the probability measure of Brownian motion and ℱ t a filtration generated by all the Brownian motions b t k on [t, ∞). If f : Ω → H is a random variable, mapping Ω into a Hilbert space H, for example, \(H = {L}^{2}({\mathbb{T}}^{3})\), then L 2(Ω, ℱ, ℙ; H) is a Hilbert space with norm:
where E denotes the expectation with respect to ℙ and f # ℙ denotes the pull back of the measure ℙ to H. A stochastic process f t in ℒ 2 = L 2([0, T]; L 2(Ω, ℱ, ℙ; H)) has the norm
and f t has the following properties; see [51].
Definition 4.1.
-
1.
f(t, ω) : ℝ + ×Ω → ℝ is measurable with respect to ℬ ×ℱ where ℬ is the σ-algebra of the Borel sets on [0, ∞), ω ∈ Ω.
-
2.
f(t, ω) is adapted to the filtration ℱ t .
-
3.
$$E\left ({\int \nolimits \nolimits }_{0}^{T}{f}^{2}(t,\omega )\mathrm{d}t\right ) < \infty.$$
We are mostly interested in the Hilbert spaces \(H = {H}^{m}({\mathbb{T}}^{3}) = {W}^{(m,2)}\) that are the Sobolev spaces based on L 2 with the Sobolev norm
The corresponding norm on \({\mathcal{L}}_{m}^{2} = {L}^{2}([0,T];{L}^{2}(\Omega,\mathcal{F}, \mathbb{P};{H}^{m}({\mathbb{T}}^{3})))\) is
more information about Sobolev spaces can be found in [1]. We will abuse notation slightly in this section by writing u instead of U; see Sect. 1.4. This is done for future reference and an easier comparison with Leray’s classical estimates.
Let \(\langle \)⋅, ⋅\(\rangle \)denote the inner product on \({L}^{2}({\mathbb{T}}^{3})\). The following a priori estimates provide the foundation of the probabilistic version of Leray’s theory.
Lemma 4.1.
The L 2 norms |u| 2 (ω,t) and |∇u| 2 (ω,t) satisfy the identity
and the bounds
where λ 1 is the smallest eigenvalue of − Δ with vanishing boundary conditions on the box [0,1] 3 and h k = |h k 1∕2 | 2. U is the velocity vector from Sect. 1.4. The expectations of these norms are also bounded:
Proof.
The identity (4.1) follows from Leray’s theory and Ito’s lemma. We apply Ito’s lemma to the L 2 norm of u squared:
where k ∈ ℤ 3 and \({h}_{k}^{1/2} \in {\mathbb{R}}^{3}\). Now by use of the Navier–Stokes equation (1.21)
since the divergent-free vector u is orthogonal both to the gradient ∇ Δ − 1(trace( ∇ u)2) and u ⋅ ∇ u by the divergence theorem. Notice that the inner product (average) of u and the stirring force f in (1.21) vanish, \(\langle u,f\rangle =\bar{ u} \cdot f = 0\), so f can be omitted in the computation. The first term in the last expression is obtained by integration by parts. This is the identity (4.1). The inequality (4.2) is obtained by applying Poincaré’s inequality
where λ1 is the smallest eigenvalue of − Δ with vanishing boundary conditions on the cube [0, 1]3.Footnote 1 By Poincaré’s inequality
Solving the inequality gives (4.2). Equation (4.3) is obtained by integrating (4.1)
and dropping | u − U | 2 2(t) > 0, by use of (1.37).
Finally we take the expectations of (4.2) and (4.3) to obtain, respectively, (4.4) and (4.5), using that the function ⟨u, h k 1 ∕ 2 e k ⟩(ω, t) is adapted to the filtration ℱ t .
The following amplification of Leray’s a priori estimates will play an important role in the a priori estimates of the solution of the stochastic Navier–Stokes equation below.
Lemma 4.2.
Let \({u}_{ \frac{1} {2B} } = u(x,t + \frac{1} {2B})\) denote the translation of u in time by the number \(\frac{1} {2B}\) . Then the L 2 norms of the differences \(\vert u - {u}_{ \frac{1} {2B} }{\vert }_{2}(\omega,t)\) and \(\vert \nabla u -\nabla {u}_{ \frac{1} {2B} }{\vert }_{2}(\omega,t)\) satisfy the identity
and the bounds
where λ 1 is the smallest eigenvalue of − Δ with vanishing boundary conditions on the box [0,1] 3 and h k = |h k 1∕2 | 2 . The expectations of these norms are also bounded
by the expectations of the initial data of the differences.
The proof of this lemma is analogous to the proof of Lemma 4.1 and can be found in [17].
Remark 4.1.
Notice that in the notation of Sect. 1.4 \(\vert U - {U}_{ \frac{1} {2B} }{\vert }_{2}^{2} = \vert u - {u}_{ \frac{1} {2B} }{\vert }_{2}^{2}\) because the constant velocity U cancels out.
4.2 The A Priori Estimate of the Turbulent Solutions
The mechanism of the turbulence production are fast oscillations driving large turbulent noise that was initially seeded by small white noise, as explained in the previous section. These fast oscillations are generated by the fast constant flow U = U 1, where we have dropped the subscript 1, and the flow is rotating with amplitude A and angular velocity Ω. The frequency of these oscillations increases with U and AΩ. The bigger U and AΩ are the more efficient this turbulence production mechanism becomes.
In this section we will establish an a priori estimate on the norm of the turbulent solution that allows us to extend the local existence and uniqueness to the whole real-time axis. Thus the a priori estimates suffice to give global existence and uniqueness. We recall the oscillatory kernel (1.34) from Sect. 1.4:
The imaginary part of the argument of the exponential creates oscillations and as U 1 and AΩ become larger these oscillations become faster. We take advantage of this mechanism to produce the a priori estimates.
Next lemma plays a key role in the proof of the useful estimate of the turbulent solution. It is a version of the Riemann–Lebesgue lemma which captures the averaging effect (mixing) of the oscillations.
Lemma 4.3.
Let the Fourier transform in time be
where \(A({k}_{2},{k}_{3}) = A\sqrt{{k}_{2 }^{2 } + {k}_{3 }^{2}}\) and w = w(k,t), k = (k 1 ,k 2 ,k 3 ), is a vector with three components. If T is an even integer multiple of \(\frac{1} {{k}_{1}U+A({k}_{2},{k}_{3})\Omega }\) , then
where
and #w satisfies the estimate
Proof.
The proof is similar to the proof of the Riemann–Lebesgue lemma for the Fourier transform in time, let B(k) = k 1 U + A(k 2, k 3)Ω:
where we have used in the last step that w is a periodic function on the interval [0, T]. Taking the average of the first and the last expression we get
Now
by the mean-value theorem.
Corollary 4.1.
If T is not an even integer multiple of \(\frac{1} {B(k)} = \frac{1} {{k}_{1}U+A({k}_{2},{k}_{3})\Omega }\) , then
where \(\tilde{w}\) satisfies the estimate
Proof.
The proof is the same as of the lemma except for the step
The lemma allows us to estimate the Fourier transform (in t) of w in terms of the time derivative of w, with a gain of (k 1 U + A(k 2, k 3)Ω) − 1. Below we will use it in an estimate showing that the limit of #w is zero when | B(k) | = | (k 1 U + A(k 2, k 3)Ω) | → ∞.
Lemma 4.4.
The integral
where B(k) = k 1 U + A(k 2 ,k 3 )Ω, is bounded by
for 0 ≤ p < 2, where C is a constant. In particular,
Proof.
We estimate the integral
where
is the value of k where the integrand achieves its maximum.
The rotation can resonate with the uniform (linear) flow due to the nonlinearities in the Navier–Stokes equation. The following lemma restricts the values of velocity coefficients so that no resonance occurs.
Lemma 4.5.
Suppose that for k 1 < 0 and \(\frac{\sqrt{{k}_{2 }^{2 }+{k}_{3 }^{2}}} {\vert {k}_{1}\vert } \neq 0\:\:\mathrm{or}\:\:\infty,\) the constants U, A, and Ω satisfy the non-resonance condition
where C is a constant and 0 < r < 1; then for all k = (k 1 ,k 2 ,k 2 )≠0,
and
Moreover,
Proof.
If k 1 > 1, then
so (4.22) and (4.23) hold. If k 1 < 0, then by (4.21)
and
if | k 1 | → ∞. If on the other hand | k 1 | < ∞ when | k | → ∞ then (4.23) also holds. When k 1 = 0, (4.22) and (4.23) are obvious and also if k 2 = k 3 = 0.
The lower bound (4.24) is read of
when k 1 ≥ 1. Then it is either U or AΩ. When k 1 = 0 then it is AΩ and by (4.21), when k 1 ≤ − 1, it is greater than or equal CAΩ.
The next question to ask is in which space do the turbulent solutions live? This was pointed out by Onsager in 1945 [53]. He pointed out that if the solutions satisfy the Kolmogorov scaling down to the smallest scales, they must be Hölder continuous function with Hölder exponent 1/3. In three dimensions this means that they live in the Sobolev space \({H}^{\frac{11} {6} +\epsilon }\) based on \({L}^{2}({\mathbb{T}}^{3})\).
If \(\frac{q} {p}\) is a rational number let \({\frac{q} {p}}^{+}\) denote any real number \(s > \frac{q} {p}\).
Theorem 4.1.
Let the velocity U = U 1 of the mean flow and the product AΩ of the amplitude A and the frequency Ω of the rotation be sufficiently large, in the uniform rotating flow (1.19), with U, AΩ also satisfying the non-resonance conditions (4.21). Then the solution of the integral equation (1.32) is uniformly bounded in \({\mathcal{L}}_{{\frac{11} {6} }^{+}}^{2},\)
where B = min (|U|,AΩ,CAΩ) is large, δ small, and C and C′ are constants.
Corollary 4.2 (Onsager’s Observation).
The solutions of the integral equation (1.32) are Hölder continuous with exponent 1∕3.
Remark 4.2.
The estimate (4.25) provides the answer to the question we posed in Sect. 1.4 how fast the coefficients h k 1 ∕ 2 had to decay in Fourier space. They have to decay sufficiently fast for the expectation of the \({H}^{{\frac{11} {6} }^{+} } =\ {W}^{({\frac{11} {6} }^{+},\ 2) }\) Sobolev norm of the initial function u 0, to be finite. This expectation appear on the right-hand side of (4.25). In other words the \({\mathcal{L}}_{{\frac{11} {6} }^{+}}^{2}\) norm of the initial function u 0 has to be finite.
The proof of the theorem involves long estimates and can be found in [17]. An outline of the proof is given in Appendix 4.3.
We consider the integral equation
where B(k) = Uk 1 + A(k 2, k 3)Ω.
Lemma 4.6.
The initial condition \((u - {u}_{ \frac{1} {2B} })(0)\) satisfies the estimate
Proof.
We use the integral equation
where B(k) = Uk 1 + A(k 2, k 3)Ω. At t = 0,
by the same estimates as above.
Lemma 4.7.
The identity (4.1) in Lemma 4.1 can be modified for a > 0
and produces the estimates
and
where λ 1 is the smallest eigenvalue of − Δ with vanishing boundary conditions on the box [0,1] 3 and h k = |h k 1∕2 | 2.
Proof.
We multiply the identity (4.1) in Lemma 4.1 by eνat to get (4.27). Then integration gives the equality
Now substituting the estimate (4.2), from Lemma 4.1, for | u | 2 2 on the right-hand side gives the two inequalities (4.28) and (4.29) as in Lemma 4.1.
Lemma 4.8.
The functions H,K, and L in the proof of Theorem 4.1 satisfy the estimate
with B = min (U,AΩ,CAΩ).
The proof of the lemma involves long formulas for H, K, and L and can be found in [17].
Remark 4.3.
Corollary 4.2 is the resolution of a famous question in turbulence, for the swirling flows: Is turbulence always caused by the blow up of the velocity u? The answer according to Theorem 4.1 is no; the solutions are not singular. However, they are not smooth either, contrary to the belief, stemming from Leray’s theory [42], that if solutions are not singular then they are smooth. By Corollary 4.2 the solutions are Hölder continuous with exponent 1 ∕ 3 in three dimensions. This confirms an observation made by Onsager [54] in 1945. In particular the gradient ∇ u and vorticity ∇ ×u are not continuous in general as discussed in Sect. 3.7.
Remark 4.4.
U and AΩ do not have to be made very large for the estimate (4.25) to be satisfied, because B(k) → ∞ as | k | → ∞. How big U and AΩ have to be for (4.25) to hold is probably best answered by a numerical simulation.
We can now prove that \(\mathrm{{ess\ sup}}_{t\in [0,\infty )}\|u{(t)\|}_{{\frac{11} {6} }^{+}}^{2}\) is bounded with probability close to one.
Lemma 4.9.
For all ε > 0 there exists an R such that
Proof.
By Chebyshev’s inequality and the estimate (4.25) we get that
for R sufficiently large.
4.3 Existence Theory of the Stochastic Navier–Stokes Equation
In this section we prove the existence of the turbulent solutions of the initial value problem (1.23). The following theorem states the existence of turbulent solutions in three dimensions. First we write the initial value problem (1.23) as the integral equation (4.32)
Here eKt is the oscillatory heat kernel (1.33) and
the A t ks being the oscillatory Ornstein–Uhlenbeck-type processes from (1.34).
Theorem 4.2.
If the uniform flow U and product of the amplitude and frequency AΩ, of the rotation, are sufficiently large, B = min (|U|,AΩ,CAΩ), δ is small and the non-resonance conditions (4.21) are satisfied, so that the a priori bound (4.25) holds, then the integral equation (4.32) has unique global solution u(x,t) in the space \(C([0,\infty );{L}^{2}(\Omega,\mathcal{F}, \mathbb{P};{H}^{{\frac{11} {6} }^{+} }))\) , u is adapted to the filtration generated by the stochastic process
and
This theorem is a standard application of the contraction mapping principle to prove global existence and uniqueness. Then the unique local solution is extended to the whole positive time axis by use of the a priori bound (4.25). A detailed proof can be found in [17].
We now add the initial condition u(x, 0) = u 0(x), with mean zero, to the integral equation (4.32).
Theorem 4.3.
If the uniform flow U and the product of the amplitude AΩ and frequency of the rotation, B = min (|U|,AΩ,CAΩ), are sufficiently large, δ small, and the non-resonance conditions (4.21) are satisfied, so that the a priori bound (4.25) holds, then the integral equation
where e Kt is the oscillating kernel in (1.33), has unique global solution u(x,t) in the space \(C([0,\infty );{L}^{2}(\Omega,\mathcal{F}, \mathbb{P};{H}^{{\frac{11} {6} }^{+} }))\) , u is adapted to the filtration generated by the stochastic process
and
The proof of the theorem is exactly the same as the proof of Theorem 4.2 once the a priori bound (4.25) is established. A proof can be found in [17].
Corollary 4.3.
For any initial data \({u}^{0} \in \dot{ {L}}^{2}({\mathbb{T}}^{3})\) , the L 2 space with mean zero, and any t 0 > 0, there exists a mean flow U, an amplitude and angular velocity AΩ, and δ small, such that (4.34) has a unique solution in \(C([{t}_{0},\infty );{L}^{2}(\Omega,\mathcal{F}, \mathbb{P};{H}^{{\frac{11} {6} }^{+} }))\).
Proof.
For t > 0, eKt ∗ u 0(x) is smooth. Now apply Theorem 4.3.
Next we prove a Gronwall estimate that can be use to prove local (in t) stability and irreducibility; see [17].
Lemma 4.10.
Let u be a solution of (4.32) with an initial function u 0 (x,t) = ∑ k≠0 h k 1∕2 A t k e k and initial condition u 0 (x) and y a solution of
with initial condition y 0 (x), then
where C 1 and C 2 are constants and δ can be made arbitrarily small. The A t k s are the oscillatory Ornstein–Uhlenbeck-type processes (1.35) and e Kt is the oscillatory kernel in (1.33).
Proof.
We subtract the integral equation for y from that of u:
Thus
where w = u − y and α = u + y. Now the same estimates as in Theorem 4.1 give
Then Grönwall’s inequality gives (4.37).
Notes
- 1.
We should subtract the mean from u in Poincaré’s inequality because of the periodic boundary conditions, but the mean just washes out in the estimates.
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© 2013 Björn Birnir
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Birnir, B. (2013). Existence Theory of Swirling Flow. In: The Kolmogorov-Obukhov Theory of Turbulence. SpringerBriefs in Mathematics. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-6262-0_4
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